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Расчет нестационарного тепловлажностного режима в различных климатических зонах влажности РоссииThis paper presents mathematical modeling of unsteady-state moisture regime of various enclosing

Discrete-Continuous Approach to the Moisture Transfer in Building EnclosuresIn the field of the moisture regime of the enclosing structure, there are methods for assessing

Heat and Moisture Regimes in the Facade Thermal Insulation Composite System with Polystyrene Insulation of mineral wool. Thus, the moisture regime process of enclosing structures which contain polystyrene

Soil And Forest Characteristics Of The Sample Plots In The Conditions Of Sod-Podzolic Soils Of The Forest Experimental Garden, Russian State Agrarian University - Moscow Timiryazev Agricultural Academy processes of soil formation the formation of pure coniferous and deciduous, and mixed forest stands in terms

The Impact of Climatic Factors on CО2 Emissions from Soils of Middle-Taiga Forests in Central Siberia: Emission as a Function of Soil Temperature and Moisture by the moisture conditions and only secondarily by the temperature regime and ecosystem type. The effect

THE MOISTURE REGIME OF ENCLOSING STRUCTURES IN DIFFERENT CONSTRUCTION AREAS. Algorithm for calculating the moisture regime according to the proposed mathematical model is given

Heat and Moisture Transfer in Building Enclosing Structures. Equations of steady-state moisture regime usually can be usually solved by analytical expressions

Effect of sprinkler irrigation on the properties of leached chernozem and the yield of Bromopsis inermis Leyss. in the Southern Cis-Ural-Ural forest-steppe. The study analysed changes in the soil's agrophysical and chemical properties. As a result

Assessment of Central Siberia Forest Ecosystems Sustainability to Forest Fires: Academic Research Outcomes been remained as the main natural factor devastating forest ecosystems and outlining the status

DERIVATION OF THE EQUATION OF UNSTEADY-STATE MOISTURE BEHAVIOUR IN THE ENCLOSING STRUCTURES OF BUILDINGS USING A DISCRETE-CONTINUOUS APPROACHTwo differential equations of moisture transfer based on the theory of moisture potential have been

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